{"title":"气候变化和人类在阿塔卡马沙漠极度干旱核心的占领","authors":"C. Latorre","doi":"10.4316/GEOREVIEW.2016.0.0.329","DOIUrl":null,"url":null,"abstract":"Significant changes in available moisture have occurred in the hyperarid Atacama Desert throughout the late Quaternary. Paleorecords show that areas in the adjacent high Andes and western Altiplano have experienced significant increases in rainfall, likely the result of intensified summer systems associated with the South American Summer Monsoon, tropical Pacific sea-surface temperature gradients and the mean position of the Intertropical Convergence Zone","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"49"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Climate change and human occupation in the hyperarid core of the Atacama Desert\",\"authors\":\"C. Latorre\",\"doi\":\"10.4316/GEOREVIEW.2016.0.0.329\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Significant changes in available moisture have occurred in the hyperarid Atacama Desert throughout the late Quaternary. Paleorecords show that areas in the adjacent high Andes and western Altiplano have experienced significant increases in rainfall, likely the result of intensified summer systems associated with the South American Summer Monsoon, tropical Pacific sea-surface temperature gradients and the mean position of the Intertropical Convergence Zone\",\"PeriodicalId\":30470,\"journal\":{\"name\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"volume\":\"26 1\",\"pages\":\"49\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4316/GEOREVIEW.2016.0.0.329\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.329","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Climate change and human occupation in the hyperarid core of the Atacama Desert
Significant changes in available moisture have occurred in the hyperarid Atacama Desert throughout the late Quaternary. Paleorecords show that areas in the adjacent high Andes and western Altiplano have experienced significant increases in rainfall, likely the result of intensified summer systems associated with the South American Summer Monsoon, tropical Pacific sea-surface temperature gradients and the mean position of the Intertropical Convergence Zone
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